abstract: ABSTRACT The Wesley Bolin Memorial Plaza is located across the street from the state capitol building in Phoenix, Arizona. Here, pieces of Arizona’s history are commemorated through monuments and memorials. Monuments and memorials reflect how people have conceived their collective identity, especially when those choices are made in public spaces. The markers in the Wesley Bolin Plaza reflect the changing identity of Arizonans, both locally and in connection to national identity. Over time, they have become crucial to shaping the landscape and the historical memory of the city, state, or country. Of note, the memorials on the Arizona State Capitol grounds are unique in how they are placed all together in a park directly across the street. In 1976, the Wesley Bolin Memorial Plaza emerged through a conversation with broader currents in the region’s and nation’s history. Over time, the plaza has become a sacred space because so many of its memorials include relics and artifacts, or list the names of those who have lost their lives in their service to Arizona. In these ways the plaza became a landscape of memory where visitors come to remember and honor those people and parts of Arizona history. The memorial plaza also influences Arizonans’ knowledge of history. It engenders a local as well as a national loyalty and identity in its citizens and visitors. By researching the history of several of the prominent monuments and memorials in the plaza, I discovered a rich history and an intriguing story behind each one that is built. Most monuments and memorials are commemorating complex events or people in history, yet have only short inscriptions on them. As a result, much of the historical narrative, complexities, and symbolism can be lost. My purpose is to tell the story of the plaza, these memorials, and their history; highlighting their significance to Arizonans and explaining how the monuments and memorials fit into the larger story of historical commemoration. / Dissertation/Thesis / Masters Thesis History 2019

The Golden Throne Quadrangle is located within Capitol Reef National Park, south-central Utah. Geologic mapping of this 1:24,000 scale 7.5 minute quadrangle began in 2003 as the National Parks Service desired to have geologic maps at this scale produced within the park. Stratigraphically, ten bedrock formations and ten Quaternary deposits are exposed within the Golden Throne Quadrangle. Geologic formations range in age from Permian to Jurassic. This map contains details not included on previous geologic maps including; the members of the Carmel, Chinle, and Moenkopi Formations. Additionally, the Page Sandstone is herein mapped as an independent unit. Structurally the Golden Throne Quadrangle encompasses most of the southern quarter of the Miners Mountain uplift. The crest of this southwest verging uplift is cut by the left-lateral strike-slip Teasdale Fault zone. Preparation of a cross-section through the axis of the uplift within the quadrangle has not permitted the use of usual faulting and folding mechanisms (i.e. fault-bend folds and fault-propagation folds) for the creation of the uplift. Two structural models can account for the geometries observed in the field. The first model is a high angle reverse basement fault; the second model is a fold over an inverted basin. The Jurassic Page Sandstone, in the Golden Throne Quadrangle, is composed of the Harris Wash and Thousand Pockets Members, which are divided by the Judd Hollow Tongue, a member of the overlying Carmel Formation It represents an erg deposit and is primarily composed of eolian sandstone. Study of the formation within the Golden Throne Quadrangle helped in the understanding of its local characteristics. Previous research has helped to develop a regional stratigraphic framework for the Page Sandstone. This study cannot be easily incorporated into the regional framework of previous studies. In order to fully understand the sedimentology of the Page Sandstone additional research will need to be accomplished.

The site is in a garage area in the state capitol complex, Austin Texas. Even though this place is located near by important government facilities and public park and links between UT Campus and Central Business District, there are no people who enjoy the place because there are no function except parking. There are just authoritative and mono-cultural office buildings and boring parking buildings. On the street, there are no trees, retails, and galleries for pedestrians. Existing parking buildings are same type and structure. Because the city has several plans to develop this area in the future such as Waller Creek Development, UT Medical School Master Plan, and Austin's Urban Rail, you can see the importance of this area. The most critical problem is this area is cutting the relationship between UT Campus and Downtown. My question is "How can a new type of parking building contribute to make the Texas Capitol Complex good place?" So I suggest a new type of mix-used parking building. The project goal is to gather people, link separated places: The State Capitol, Waller Creek, UT Campus, CBD, intermingle different functions: garage, gallery, shop, theater, restaurant, lounge, pool, park, and then make the place more dynamic, enjoyable and energetic place. Further, I expect that Austin become interesting city to live and visit through like this new place. / text

Thesis (M.A.)--Virginia Polytechnic Institute and State University, 1994. / Vita. Abstract. Includes bibliographical references. Also available via the Internet.

Thesis (M.S.)--Brigham Young University. Dept. of Geology, 2005. / Includes bibliographical references.

Students who are engaged in their high school environment have higher graduation rates, fewer discipline problems, and lower delinquency rates. In addition, students who are connected to teachers and involved in extracurricular activities consistently experience positive outcomes. However, although the benefits of school resources such as extra-curricular activities and connections to supportive individuals during high school have been well documented, the factors influencing utilization of these resources have not yet been established. Given the known benefits of activity participation and connection to supportive individuals in school settings, and the voluntary nature of their utilization, it is important to investigate factors influencing students' decision to use these resources. The current study investigated potential barriers and facilitating factors for high school students' activity involvement and support seeking from school personnel. Survey data were collected from 1522, 9-12th grade students in four Pinellas County high schools. Questions regarding students' school, family, and social relationships were assessed via psychometrically valid scales, district records, and items created collaboratively with school district administrators for this specific project. Results were analyzed using bivariate correlations and hierarchical multiple regression. Race, free/reduced lunch status, parent involvement and psychological distress were among the strongest correlates with the support seeking outcomes whereas gender, race, free/reduced lunch status, global self worth, self esteem, antisocial peer group, and perceived school support were among the variables most strongly correlated with the activity involvement outcomes. All significant relationships found were in the predicted direction with barrier variables leading to lower levels of school engagement and facilitating factors leading to higher levels of school engagement. Contrary to the hypotheses, the selected barriers and facilitating factors did not contribute to a significant amount of variance above that accounted for by gender, race, and free/reduced lunch status. In general, males, students receiving free/reduced lunch, and black students had the lowest rates of school engagement. The current results add to existing literature by showing that students who would benefit most from positive assets such as support seeking from adults at school and activity involvement are least likely to engage in the behaviors.

Leasing has become a desirable alternative for acquiring capital equipment in the 80's. However, there are many tangible and intangible conditions that must be taken into consideration before signing a lease contract. This report presents leasing terminology, and the new tax laws that are relevant to leasing; explaining and illustrating common true lease plans on a before and after-tax basis, and finally, developing microcomputer software for the discussed true lease plans. / Master of Engineering

This paper provides a closer analysis of the discourse in doxing in a sample of digital and printed US and European media with a particular focus on the Capitol riots. The analysis centers around the following questions: How is doxing portrayed? How are its victims and perpetrators portrayed? What expressions about doxing appear depending on who performs the act versus being exposed? When it comes to how doxing is valued in the discourse, there are three categories that determine how the discourse is portrayed. (1) Who is behind the doxing? (2) who is the target of doxing? (3) What is the purpose of doxing? These categories work in symbiosis with each other. A positive notion of the doxxer, a negative notion about the person being doxxed and a justified purpose is needed for it to be valued in the discourse. Two main types of doxing could be distinguished that are framed in different ways in the discourse, doxing for malicious purposes and doxing for political purposes. In relation to the U.S capitol riots, Doxing was recontextualized. The change is explained trough (Re-) definition, a ‘theoretical legitimation’ strategy where actions are legitimized through defining an action in terms of ‘another, moralized activity’.

A new geologic map of the Deer Point 7.5' quadrangle located in the southern region of Capitol Reef National Park in south-central Utah provides stratigraphic and structural detail not previously available. The Deer Point quadrangle was mapped at a scale of 1:24,000 and is the fourth geologic map completed at this scale in Capitol Reef National Park. Twelve Quaternary units and eighteen bedrock formations and members are exposed in the Deer Point quadrangle. Bedrock formations range in age from Triassic to Cretaceous. The details not available on previous geologic maps include: four alluvial terrace units, two lacustrine units, two mass movement units, and members of the Moenkopi, Chinle, and Carmel Formations. Historically the Page Sandstone has been mapped as part of the Navajo Sandstone or the Carmel Formation. This map identifies the Page Sandstone as a separate and independent unit. The Deer Point quadrangle is cross cut by a portion of a Laramide-age, basement cored, NNW-SSE trending asymmetrical anticline called the Waterpocket Fold. Strikes and dips measured throughout the Deer Point quadrangle identify the vergence of the anticline as eastward with a maximum dip of 49˚ on the forelimb and 7˚ on the backlimb. The maximum dip on the forelimb dramatically decreases in the southern quarter of the quadrangle to 15˚.The Utah Geological Survey is mapping the Hite Crossing 30' x 60' quadrangle at a scale of 1:62.500. The Deer Point quadrangle is one of 32 quadrangles that comprise the Hite Crossing quadrangle. The Utah Geological Survey is working to establish erosion rates on the Colorado Plateau. To do this, they are dating alluvial terrace deposits. Within the Deer Point quadrangle four new terrace levels have been identified that could help with this research. Additional research could use these terrace deposits to better understand erosion rates in the Deer Point quadrangle and the broader Colorado Plateau. Numerous mass movement deposits are found within the Deer Point quadrangle. The largest has been named the Red Slide. Several aspects of the Red Slide are identified including classification, breakaway zone, source, deposit size, composition, debris flow path and depositional history. The Red Slide has been classified as a debris flow. The breakaway zone is a concave cliff 1.5 miles (2.4 km) to the west of the debris flow's present location. The flow's scarp is no longer identifiable. The source of the debris flow material is the Chinle Formation and Wingate Sandstone. The Red Slide deposit covers an area of over 16.6 million ft2 (~1.5 million m2). The toe of the debris flow is 1 mile (1.6 km) wide. The estimated maximum thickness of the debris flow is sixty meters. The Red Slide is composed of fine-grained, clay- and silt- sized material, and a small amount of angular pebble- to cobble-sized limestone clasts from the Owl Rock Member of the Chinle Formation. Boulder- to sand-sized grains from the Wingate Sandstone are scattered throughout the deposit with the larger grains forming inversely grading packages. The Red Slide likely occurred as a series of large debris flows, not one catastrophic event, although they may have occurred at about the same time.

No description available.